Northern
Christian Advocate – New York
August
25, 1881
VOLCANO
There
are reports of a volcanic eruption in Idaho.
August 9th a column of fire and smoke is said to have
burst from a mountain summit about 1000 feet above the south fork of the
Clearwater, about 20 miles east from Mt. Idaho; the smoke continued to
pour forth in great volume and to rise several hundred feet.
A rock of considerable size was also thrown a number of miles
from the mountain’s base. There
were in t he region distinct evidences of former volcanic action.
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Daily
Gazette – New Jersey
August
18, 1881
A
VOLCANO IN IDAHO
A
dispatch from Lewiston, Idaho, says that there was a volcanic eruption
in the mountain south of the South Fork of the Clearwater, about twenty
miles east of Mt. Idaho, on the 9th instant.
The mountain sent forth a column of fire and smoke several
hundred feet in height, and a rock, which fell at a distance of several
miles from the place of eruption. The
shock was distinctly felt at Mt. Idaho, on the extreme west of the Camas
Prairie, and at the mouth of Salmon River, a distance of about 75 miles.
Later
news from Camas Prairie says that a column of smoke is coming from the
opening, which is distinctly visible from the prairie.
No one as yet has approached the place.
Evidence of volcanic action at some former periods exist in many
places in the immediate vicinity. So
far as appears the opening is less than a thousand feet above the bed of
the South Fork of the Clearwater, and within three miles of the Milner
trail, between Mt. Idaho and Florence.
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The
Owyhee Avalanche
September
10, 1881
IDAHO
VOLCANO
The
Nez Perce News of the 1st instant says:
“Our big brother, Col. F.J. Parker, returned from the inside last
night, and says that the supposed volcano is simply a chemical eruption at the
head of a ridge of high altitude known as Devil’s back, a divide between the
waters of the Salmon and Clearwater rivers.
The trees on the mountain sides are shattered into kindling wood by the
force of the explosion, and also set the woods on fire.
The formation in the vicinage of the eruption is quartzite and
limestone, and is terribly broken up. There
were two explosions, the last twenty hours after the other, but not so
loud.”
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